Page:The cruise of the Corwin.djvu/147

sheet, has been light, sculpturing the mountains into shallow, short valleys and round ridges, mostly broad-backed. The valleys, for the most part, are not cut down to the sea. The shore seems to have been cut off by the glacier sheet that occupied the sea, after it was too shallow to flow over the angle of land formed by East Cape. This overflow is well-marked, fifteen to twenty-five miles northwest of the Cape, in the trends of the ridges and valleys as far back as I could see, that is, about twenty-five miles from the shore. The north wind is, and has been, blowing for twenty-four hours, and we fear that we will soon meet with the drifting ice from the main polar pack.

We arrived here about eight this morning to meet the search party that we landed about a month ago, near Koliuchin Island. They had been waiting for us nearly two weeks. We were unable to land on account of the stormy weather, but after waiting about two hours we saw them making their way out to the edge of the drift ice, which extended about three miles from shore, and after a good deal of difficulty they reached the steamer in safety. The air